B42A-03
Estimating Pan Arctic Net Ecosystem Exchange using Functional Relationships with Air temperature, Leaf Area Index and Photosynthetic Active Radiation

Thursday, 17 December 2015: 10:50
2006 (Moscone West)
Herbert Mbufong1, Antonin Kusbach2, Magnus Lund3, Andreas Persson2, Torben R Christensen4, Mikkel P Tamstorf1,5 and John Connolly6, (1)Aarhus University, Aarhus, Denmark, (2)Lund University, Department of Physical Geography and Ecosystem Science, Lund, Sweden, (3)Aarhus University, Department of Bioscience, Aarhus, Denmark, (4)Lund University, Physical Geography and Ecosystem Science, Lund, Sweden, (5)Aarhus University, Arctic Research Center, Aarhus, Denmark, (6)DCU St. Patrick's Campus, Department of Geography, Dublin, Ireland
Abstract:
The high variability in Arctic tundra net ecosystem exchange (NEE) of carbon (C) is often attributed to the high spatial heterogeneity of Arctic tundra. Current models of carbon exchange thus handle the Arctic as either a single or few ecosystems, responding to environmental change in the same manner. In this study, we developed and tested a simple NEE model using the Misterlich light response curve (LRC) function with photosynthetic photon flux density (PPFD) as the main driving variable. Model calibration was carried out with eddy covariance carbon dioxide data from 12 Arctic tundra sites. The model input parameters (fcsat, Rd and α) were estimated as a function of air temperature and leaf area index (LAI) and represent specific characteristics of the NEE-PPFD relationship. They describe the saturation flux, dark respiration and initial light use efficiency, respectively. While remotely sensed LAI is readily available as a MODIS Terra product (MCD15A3), air temperature was estimated from a direct relationship with MODIS land surface temperature (MOD11A2, LST). Therefore, no specific knowledge of the vegetation type is required. Preliminary results show the model captures the spatial heterogeneity of the Arctic tundra but so far, overestimates NEE on all 17 test sites which include heaths, bogs, fens, and tussock tundra vegetation. The final updated results and error assessment will be presented at the conference in December.